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AGREEMENT WITH THE EQUATIONS IN TWO DIMENSIONS

The 2-D system derived by Artley 1992 is a set of four equations with four unknowns. It can be retrieved by replacing the vectorial ray parameters with their scalar form (since the vectors are now in a common plane). The first relation of system (14) then becomes  
 \begin{displaymath}
\xi(p_g,t_g) - \xi(p_s,t_{sg}-t_g) = 2h ,\end{displaymath} (18)
where h is the half offset. The fourth relation becomes  
 \begin{displaymath}
\frac{\sin \theta(p_0,t_0)}{v} \left( \cos \theta(p_s,t_s)
 ...
 ...
 + \frac{\sin \theta(p_g,t_g)}{v} \right) \cos \theta(p_0,t_0)\end{displaymath} (19)
and can be simplified to  
 \begin{displaymath}
\sin( \theta(p_0,t_0) - \theta(p_s,t_s) ) =
 \sin( \theta(p_g,t_g) - \theta(p_0,t_0) ) .\end{displaymath} (20)
Finally, we obtain the bisection condition as shown by Artley 1992, as follows:  
 \begin{displaymath}
\theta(p_0,t_0) = \frac{1}{2}\left[ \theta(p_s,t_s)
 + \theta(p_g,t_g) \right] .\end{displaymath} (21)


previous up next print clean
Next: CONCLUSION Up: Artley et al.: Equations Previous: Solving the system
Stanford Exploration Project
11/17/1997